Article ID | Journal | Published Year | Pages | File Type |
---|---|---|---|---|
5468806 | Applied Clay Science | 2016 | 9 Pages |
Abstract
Viscosity measurements show that for both CMC solutions and bentonite-CMC dispersions sudden changes in viscosity occur as the temperature increases. The viscosity is found to decrease below a critical temperature which corresponds to a cloud point or gelation temperature. Above this later, the viscosity increases dramatically with temperature. Hydrophobic interaction is postulated to be the cause of gelation.
Related Topics
Physical Sciences and Engineering
Earth and Planetary Sciences
Geochemistry and Petrology
Authors
Abdelhakim Benslimane, Ilies Mohamed Bahlouli, Karim Bekkour, Dalila Hammiche,